River‐groundwater interactions are at the core of a wide range of major contemporary
challenges, including the provision of high‐quality drinking water in sufficient quantities, the …

Rivers are important ecosystems under continuous anthropogenic stresses. The hyporheic
zone is a ubiquitous, reactive interface between the main channel and its surrounding …

In terms of the research on groundwater–surface water heat-tracing methods, investigation
of the interactions within the compound system of the groundwater–surface water–hyporheic …

Using heat as a tracer to estimate the vertical streambed fluxes (VSFs) and sediment thermal
properties, the choice of mathematical models of heat transport is critical for the accuracy of …

As a natural tracer, heat has some remarkable advantages over competing test methods and
has become a popular and widely used tool for quantifying streambed fluxes. In recent …

Heat as a tracer has received increasing attention in recent decades and has become a
popular and widely used tool for quantifying streambed fluxes, among many other …

We present and demonstrate a recursive‐estimation framework to infer groundwater/surface‐
water exchange based on temperature time series collected at different vertical depths …

Interactions between groundwater and surface water sustain groundwater-dependent
ecosystems and regulate river temperature and biogeochemical cycles, amongst many other …

Surface water infiltration from ephemeral dryland streams is particularly important in
hyporheic exchange and biogeochemical processes in arid and semi-arid regions …

A fundamental assumption in numerous studies of heat transfer in porous media is local
thermal equilibrium (LTE), which assumes that the temperature of the porous media at the …